Zobrazeno 1 - 3
of 3
pro vyhledávání: '"Dolati A.[2]"'
Autor:
Saccani E.[1], Delavari M.[2], Dolati A.[2], Pandolfi L.[3, Barbero E.[1], Tassinari R.[1], Marroni M.[3
Publikováno v:
Journal of Asian earth sciences 228 (2022). doi:10.1016/j.jseaes.2022.105141
info:cnr-pdr/source/autori:Saccani E.[1], Delavari M.[2], Dolati A.[2], Pandolfi L.[3,4], Barbero E.[1], Tassinari R.[1], Marroni M.[3,4]/titolo:Geochemistry of basaltic blueschists from the Deyader Metamorphic Complex (Makran Accretionary Prism, SE Iran): New constraints for magma generation in the Makran sector of the Neo-Tethys/doi:10.1016%2Fj.jseaes.2022.105141/rivista:Journal of Asian earth sciences/anno:2022/pagina_da:/pagina_a:/intervallo_pagine:/volume:228
info:cnr-pdr/source/autori:Saccani E.[1], Delavari M.[2], Dolati A.[2], Pandolfi L.[3,4], Barbero E.[1], Tassinari R.[1], Marroni M.[3,4]/titolo:Geochemistry of basaltic blueschists from the Deyader Metamorphic Complex (Makran Accretionary Prism, SE Iran): New constraints for magma generation in the Makran sector of the Neo-Tethys/doi:10.1016%2Fj.jseaes.2022.105141/rivista:Journal of Asian earth sciences/anno:2022/pagina_da:/pagina_a:/intervallo_pagine:/volume:228
The North Makran Domain in the Makran Accretionary Prism consists of an imbricate stack of Mesozoic Neo Tethyan ophiolitic and metaophiolitic units. The Deyader Complex is an important metamorphic unit of this Domain and includes tectonic slices of H
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3184f23ae8855bb8dd892e66dc759931
https://publications.cnr.it/doc/466664
https://publications.cnr.it/doc/466664
Autor:
Barbero E.[1], Delavari M.[2], Dolati A.[2], Vahedi L.[2], Langone A.[3], Marroni M.[4, Pandolfi L.[4, Zaccarini F.[6] Saccani E.[1]
Publikováno v:
Minerals, Vol 10, Iss 1100, p 1100 (2020)
Minerals (Basel) 10 (2020): 1–36. doi:10.3390/min10121100
info:cnr-pdr/source/autori:Barbero E.[1], Delavari M.[2], Dolati A.[2], Vahedi L.[2], Langone A.[3], Marroni M.[4,5], Pandolfi L.[4,5], Zaccarini F.[6] Saccani E.[1]/titolo:Early cretaceous plume-ridge interaction recorded in the band-e-zeyarat ophiolite (North Makran, Iran): New constraints from petrological, mineral chemistry, and geochronological data/doi:10.3390%2Fmin10121100/rivista:Minerals (Basel)/anno:2020/pagina_da:1/pagina_a:36/intervallo_pagine:1–36/volume:10
Minerals
Volume 10
Issue 12
Minerals (Basel) 10 (2020): 1–36. doi:10.3390/min10121100
info:cnr-pdr/source/autori:Barbero E.[1], Delavari M.[2], Dolati A.[2], Vahedi L.[2], Langone A.[3], Marroni M.[4,5], Pandolfi L.[4,5], Zaccarini F.[6] Saccani E.[1]/titolo:Early cretaceous plume-ridge interaction recorded in the band-e-zeyarat ophiolite (North Makran, Iran): New constraints from petrological, mineral chemistry, and geochronological data/doi:10.3390%2Fmin10121100/rivista:Minerals (Basel)/anno:2020/pagina_da:1/pagina_a:36/intervallo_pagine:1–36/volume:10
Minerals
Volume 10
Issue 12
The North Makran domain (southeast Iran) is part of the Makran accretionary wedge and consists of an imbricate stack of continental and Neo-Tethyan oceanic tectonic units. Among these, the Band-e-Zeyarat ophiolite consists of (from bottom to top): ul
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4c4c0c206a25ec1a9e4aa5ae8504a94e
http://hdl.handle.net/11392/2432003
http://hdl.handle.net/11392/2432003
Autor:
Barbero E.[1], Delavari M.[2], Dolati A.[2], Saccani E.[1], Marroni M.[3, Catanzariti R.[4], Pandolfi L.[3
Publikováno v:
Journal of Asian earth sciences 195 (2020): 1–26. doi:10.1016/j.jseaes.2020.104306
info:cnr-pdr/source/autori:Barbero E.[1], Delavari M.[2], Dolati A.[2], Saccani E.[1], Marroni M.[3,4], Catanzariti R.[4], Pandolfi L.[3,4]/titolo:The Ganj Complex reinterpreted as a Late Cretaceous volcanic arc: Implications for the geodynamic evolution of the North Makran domain (southeast Iran)/doi:10.1016%2Fj.jseaes.2020.104306/rivista:Journal of Asian earth sciences/anno:2020/pagina_da:1/pagina_a:26/intervallo_pagine:1–26/volume:195
info:cnr-pdr/source/autori:Barbero E.[1], Delavari M.[2], Dolati A.[2], Saccani E.[1], Marroni M.[3,4], Catanzariti R.[4], Pandolfi L.[3,4]/titolo:The Ganj Complex reinterpreted as a Late Cretaceous volcanic arc: Implications for the geodynamic evolution of the North Makran domain (southeast Iran)/doi:10.1016%2Fj.jseaes.2020.104306/rivista:Journal of Asian earth sciences/anno:2020/pagina_da:1/pagina_a:26/intervallo_pagine:1–26/volume:195
The North Makran domain (southeast Iran) is part of the Makran accretionary wedge and consists of an imbricate stack of continental and oceanic tectonic units. Among these, the Ganj Complex was up to now regarded as an ophiolite unit. This Complex is
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2df655d0b9c068201b522be031ba05cf
https://doi.org/10.1016/j.jseaes.2020.104306
https://doi.org/10.1016/j.jseaes.2020.104306
